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Geobiology of Andean Microbial Ecosystems Discovered in Salar de Atacama, Chile

Authors :
Adrian Turjanski
Natalia C. Muñoz-Herrera
Daniel Gustavo Poire
Manuel Contreras
Agustina I. Lencina
Maria Eugenia Farias
Federico A. Vignale
Fernando Novoa
Elizabeth Chihuailaf
Daniel Kurth
Source :
Frontiers in Microbiology, Vol 12 (2021), SEDICI (UNLP), Universidad Nacional de La Plata, instacron:UNLP, Frontiers in Microbiology
Publication Year :
2021
Publisher :
Frontiers Media SA, 2021.

Abstract

The Salar de Atacama in the Chilean Central Andes harbors unique microbial ecosystems due to extreme environmental conditions, such as high altitude, low oxygen pressure, high solar radiation, and high salinity. Combining X-ray diffraction analyses, scanning electron microscopy and molecular diversity studies, we have characterized twenty previously unexplored Andean microbial ecosystems in eight different lakes and wetlands from the middle-east and south-east regions of this salt flat. The mats and microbialites studied are mainly formed by calcium carbonate (aragonite and calcite) and halite, whereas the endoevaporites are composed predominantly of gypsum and halite. The carbonate-rich mats and microbialites are dominated by Bacteroidetes and Proteobacteria phyla. Within the phylum Proteobacteria, the most abundant classes are Alphaproteobacteria, Gammaproteobacteria and Deltaproteobacteria. While in the phylum Bacteroidetes, the most abundant classes are Bacteroidia and Rhodothermia. Cyanobacteria, Chloroflexi, Planctomycetes, and Verrucomicrobia phyla are also wellrepresented in the majority of these systems. Gypsum endoevaporites, on the contrary, are dominated by Proteobacteria, Bacteroidetes, and Euryarchaeota phyla. The Cyanobacteria phylum is also abundant in these systems, but it is less represented in comparison to mats and microbialites. Regarding the eukaryotic taxa, diatoms are key structural components in most of the microbial ecosystems studied. The genera of diatoms identified were Achnanthes, Fallacia, Halamphora, Mastogloia, Navicula, Nitzschia, and Surirella. Normally, in the mats and microbialites, diatoms form nano-globular carbonate aggregates with filamentous cyanobacteria and other prokaryotic cells, suggesting their participation in the mineral precipitation process. This work expands our knowledge of the microbial ecosystems inhabiting the extreme environments from the Central Andes region, which is important to ensure their protection and conservation.<br />Centro de Investigaciones Geológicas

Details

ISSN :
1664302X
Volume :
12
Database :
OpenAIRE
Journal :
Frontiers in Microbiology
Accession number :
edsair.doi.dedup.....05b2347e154c122c27aa8e7c0a3fe2ad
Full Text :
https://doi.org/10.3389/fmicb.2021.762076